- The
Variscan orogeny, or
Hercynian orogeny, was a
geologic mountain-building
event caused by Late
Paleozoic continental collision between Euramerica (Laurussia)...
- Caledonian, Alleghenian,
Mauritanide and
Variscan orogenies. The
eastern portions of the
range are also
called the
Variscan Mountains. The
Central Pangean Mountains...
-
laying to the south. The
Central Pangean Mountains were
formed during the
Variscan-Alleghanian-Ouachita orogeny.
Today their remains stretch over 10,000 km...
-
Permian (more than 300
million years old) and
therefore deformed during the
Variscan Orogeny.
Parts of the
Sudetes within the
Bohemian M****if,
Giant Mountains...
- strike-slip zone.
Internal zones in
western and
eastern segments contain older Variscan igneous m****ifs
reworked in
Mesozoic thick and thin-skinned nappes. During...
-
major orogenic events occurred in this era, the
Caledonian Orogeny and the
Variscan Orogeny,
allowing a
complex geologic history to begin.
During the late...
- (2002). "Paleozoic
evolution of pre-
Variscan terranes: From
Gondwana to the
Variscan collision" (PDF).
Variscan-Appalachian dynamics: The
building of...
-
formed during the
Hercynian period. This
mountain building episode was the
Variscan orogeny,
named after Hof's
Latin name (and the
tribe of Varisci) of Curia...
-
Sudetes originated during the
Variscan orogeny and its aftermath. The
Sudetes are the
northeasternmost accessible part of
Variscan orogen as in the
North European...
- Siberia-Kazakhstania, the
latter of
which forms Laurasia and the
Uralian orogeny.
Variscan orogeny continues (these
collisions created orogenies, and
ultimately Pangaea)...
